and a pressure of 1013.25 hPa. In the
case of Iceland,
the
climate deviates significantly from these standard
atmospheric conditions.
Additionally, terrain
elevation varies considerably
across the island. Therefore, seasonal and
annual differences in
air
density from the standard value, as well as spatial variability, need to be taken into
account.
Approximate air density
can be
calculated by
assuming
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf